Crystal morphology and xrd peculiarities of brazilianite from different localities.

Bibliographic Details
Main Author: Čobić, Andrea
Publication Date: 2011
Other Authors: Zebec, Vladimir, Cipriano, Ricardo Augusto Scholz, Bermanec, Vladimir, Barreto, Sandra de Brito
Format: Article
Language: eng
Source: Repositório Institucional da UFOP
Download full: http://www.repositorio.ufop.br/handle/123456789/4140
Summary: Forty four brazilianite crystals from several localities in Brazil, Rwanda and Canada were measured on a two-circle goniometer to determine brazilianite morphology. Twenty forms were recorded; six of them have not been recorded before. All faces in the [001] zone are striated along crystallographic axis c. All striated forms in the [001] zone exhibit multiple signals. Two of the signals observed on the form {110} are always very clear. There is an exception on one crystal where just one face, (110), exhibits only one clear signal. Five groups of habits were recorded, two of them new to this mineral species. Eleven samples were examined by X-ray diffraction for calculation of the unit cell parameters yielding a=11.201(1)–11.255(2) Å, b=10.1415(5)–10.155(1) Å, c=7.0885(7)–7.119(2) Å and b=97.431(7)–97.34(1) °. All X-ray diffraction patterns show a peculiarity: some diffraction lines are widened or doubled with the appearance of additional diffraction lines systematically on lower °2Q. These diffraction lines have smaller intensities and cannot be indexed in accordance with brazilianite crystal structure.
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spelling Čobić, AndreaZebec, VladimirCipriano, Ricardo Augusto ScholzBermanec, VladimirBarreto, Sandra de Brito2014-12-11T16:40:51Z2014-12-11T16:40:51Z2011ČOBIĆ, A. et al. Crystal morphology and xrd peculiarities of brazilianite from different localities. Natura Croatica, v. 20, p. 1-18, 2011. Disponível em: <http://hrcak.srce.hr/index.php?show=clanak&id_clanak_jezik=104073&lang=en>. Acesso em: 07 out. 2014.1848-7386http://www.repositorio.ufop.br/handle/123456789/4140Forty four brazilianite crystals from several localities in Brazil, Rwanda and Canada were measured on a two-circle goniometer to determine brazilianite morphology. Twenty forms were recorded; six of them have not been recorded before. All faces in the [001] zone are striated along crystallographic axis c. All striated forms in the [001] zone exhibit multiple signals. Two of the signals observed on the form {110} are always very clear. There is an exception on one crystal where just one face, (110), exhibits only one clear signal. Five groups of habits were recorded, two of them new to this mineral species. Eleven samples were examined by X-ray diffraction for calculation of the unit cell parameters yielding a=11.201(1)–11.255(2) Å, b=10.1415(5)–10.155(1) Å, c=7.0885(7)–7.119(2) Å and b=97.431(7)–97.34(1) °. All X-ray diffraction patterns show a peculiarity: some diffraction lines are widened or doubled with the appearance of additional diffraction lines systematically on lower °2Q. These diffraction lines have smaller intensities and cannot be indexed in accordance with brazilianite crystal structure.Morfologia - mineraisMorphology - mineralsCrystalCrystal morphology and xrd peculiarities of brazilianite from different localities.info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleFull-text papers plubished in Natura Croatica can be used for personal or educational purposes only. Authors' and publisher's copyrights must be acknowledged. Fonte: Natura Croatica <http://hrcak.srce.hr/natura-croatica>. Acesso em: 08 out. 2014.info:eu-repo/semantics/openAccessengreponame:Repositório Institucional da UFOPinstname:Universidade Federal de Ouro Preto (UFOP)instacron:UFOPLICENSElicense.txtlicense.txttext/plain; charset=utf-82636http://www.repositorio.ufop.br/bitstream/123456789/4140/2/license.txtc2ffdd99e58acf69202dff00d361f23aMD52ORIGINALARTIGO_CrystalMorphologyXRD.pdfARTIGO_CrystalMorphologyXRD.pdfapplication/pdf443104http://www.repositorio.ufop.br/bitstream/123456789/4140/1/ARTIGO_CrystalMorphologyXRD.pdfa4c8c99d8489302c5cd8e312efaa3431MD51123456789/41402019-05-16 10:14:31.272oai:localhost:123456789/4140Repositório InstitucionalPUBhttp://www.repositorio.ufop.br/oai/requestrepositorio@ufop.edu.bropendoar:32332019-05-16T14:14:31Repositório Institucional da UFOP - Universidade Federal de Ouro Preto (UFOP)false
dc.title.pt_BR.fl_str_mv Crystal morphology and xrd peculiarities of brazilianite from different localities.
title Crystal morphology and xrd peculiarities of brazilianite from different localities.
spellingShingle Crystal morphology and xrd peculiarities of brazilianite from different localities.
Čobić, Andrea
Morfologia - minerais
Morphology - minerals
Crystal
title_short Crystal morphology and xrd peculiarities of brazilianite from different localities.
title_full Crystal morphology and xrd peculiarities of brazilianite from different localities.
title_fullStr Crystal morphology and xrd peculiarities of brazilianite from different localities.
title_full_unstemmed Crystal morphology and xrd peculiarities of brazilianite from different localities.
title_sort Crystal morphology and xrd peculiarities of brazilianite from different localities.
author Čobić, Andrea
author_facet Čobić, Andrea
Zebec, Vladimir
Cipriano, Ricardo Augusto Scholz
Bermanec, Vladimir
Barreto, Sandra de Brito
author_role author
author2 Zebec, Vladimir
Cipriano, Ricardo Augusto Scholz
Bermanec, Vladimir
Barreto, Sandra de Brito
author2_role author
author
author
author
dc.contributor.author.fl_str_mv Čobić, Andrea
Zebec, Vladimir
Cipriano, Ricardo Augusto Scholz
Bermanec, Vladimir
Barreto, Sandra de Brito
dc.subject.por.fl_str_mv Morfologia - minerais
Morphology - minerals
Crystal
topic Morfologia - minerais
Morphology - minerals
Crystal
description Forty four brazilianite crystals from several localities in Brazil, Rwanda and Canada were measured on a two-circle goniometer to determine brazilianite morphology. Twenty forms were recorded; six of them have not been recorded before. All faces in the [001] zone are striated along crystallographic axis c. All striated forms in the [001] zone exhibit multiple signals. Two of the signals observed on the form {110} are always very clear. There is an exception on one crystal where just one face, (110), exhibits only one clear signal. Five groups of habits were recorded, two of them new to this mineral species. Eleven samples were examined by X-ray diffraction for calculation of the unit cell parameters yielding a=11.201(1)–11.255(2) Å, b=10.1415(5)–10.155(1) Å, c=7.0885(7)–7.119(2) Å and b=97.431(7)–97.34(1) °. All X-ray diffraction patterns show a peculiarity: some diffraction lines are widened or doubled with the appearance of additional diffraction lines systematically on lower °2Q. These diffraction lines have smaller intensities and cannot be indexed in accordance with brazilianite crystal structure.
publishDate 2011
dc.date.issued.fl_str_mv 2011
dc.date.accessioned.fl_str_mv 2014-12-11T16:40:51Z
dc.date.available.fl_str_mv 2014-12-11T16:40:51Z
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dc.identifier.citation.fl_str_mv ČOBIĆ, A. et al. Crystal morphology and xrd peculiarities of brazilianite from different localities. Natura Croatica, v. 20, p. 1-18, 2011. Disponível em: <http://hrcak.srce.hr/index.php?show=clanak&id_clanak_jezik=104073&lang=en>. Acesso em: 07 out. 2014.
dc.identifier.uri.fl_str_mv http://www.repositorio.ufop.br/handle/123456789/4140
dc.identifier.issn.none.fl_str_mv 1848-7386
identifier_str_mv ČOBIĆ, A. et al. Crystal morphology and xrd peculiarities of brazilianite from different localities. Natura Croatica, v. 20, p. 1-18, 2011. Disponível em: <http://hrcak.srce.hr/index.php?show=clanak&id_clanak_jezik=104073&lang=en>. Acesso em: 07 out. 2014.
1848-7386
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